スンビン山
Sumbing
成層火山 · Indonesia · 3370m

- タイプ
- 成層火山
- 国
- Indonesia
- 地域
- Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
- 標高
- 3370m
- 座標
- -7.382, 110.075
- 最終噴火
- 1730年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Composite
- 主要岩石
- Andesite / Basaltic Andesite
地質学的概要
Gunung Sumbing is a stratovolcano that is the SE-most edifice of a chain of volcanoes in central Java that includes Sundoro and the Dieng Complex. Prominent cones are located on the N and SE flanks. An 800-m-wide summit crater is breached to the NE, but is partially filled by a lava dome that extended beyond the original crater rim. Emplacement of the dome followed the production of extensive pyroclastic flows down the NE flank. Activity reported in about 1730 CE may have produced the small phreatic craters found at the summit behind the dome.
Wikipedia の要約
英語版の要約Mount Sumbing is an active stratovolcano in Central Java, Indonesia. This volcano is symmetrical like its neighbor Mount Sindoro which lies to its northwest. Administratively, The volcano is divided between 3 regencies: Temanggung, Wonosobo, and Magelang. The only report of historical eruptions is from 1730. It has created a small phreatic crater at the summit.
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噴火履歴
詳細タイムライン
- 1730年VEI 1観測記録1730 ~ 進行中
外部リンク
⚠ 参考情報です。緊急対応には使用しないでください。